Kelvin-Helmholtz instability refers to a phenomenon that occurs when there is a velocity difference across the interface between two fluids, causing the development of waves and potential mixing. This instability is often observed in scenarios where lighter and denser fluids interact, leading to patterns such as rolling clouds or ripples on water surfaces. Understanding this instability is crucial as it ties into interfacial forces and surface tension, impacts interfacial instabilities, and plays a significant role in the broader context of multiphase flow instabilities.
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